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The 2405 Ma doleritic dykes in the Karelian Craton : A fragment of a Paleoproterozoic large igneous province. / Stepanova, A. V.; Salnikova, E. B.; Samsonov, A. V.; Larionova, Yu O.; Egorova, S. V.; Savatenkov, V. M.

In: Doklady Earth Sciences, Vol. 472, No. 1, 01.01.2017, p. 72-77.

Research output: Contribution to journal › Article › peer-review

Harvard

Stepanova, AV, Salnikova, EB, Samsonov, AV, Larionova, YO, Egorova, SV & Savatenkov, VM 2017, 'The 2405 Ma doleritic dykes in the Karelian Craton: A fragment of a Paleoproterozoic large igneous province', Doklady Earth Sciences, vol. 472, no. 1, pp. 72-77. https://doi.org/10.1134/S1028334X17010196

APA

Stepanova, A. V., Salnikova, E. B., Samsonov, A. V., Larionova, Y. O., Egorova, S. V., & Savatenkov, V. M. (2017). The 2405 Ma doleritic dykes in the Karelian Craton: A fragment of a Paleoproterozoic large igneous province. Doklady Earth Sciences, 472(1), 72-77. https://doi.org/10.1134/S1028334X17010196

Vancouver

Stepanova AV, Salnikova EB, Samsonov AV, Larionova YO, Egorova SV, Savatenkov VM. The 2405 Ma doleritic dykes in the Karelian Craton: A fragment of a Paleoproterozoic large igneous province. Doklady Earth Sciences. 2017 Jan 1;472(1):72-77. https://doi.org/10.1134/S1028334X17010196

Author

Stepanova, A. V. ; Salnikova, E. B. ; Samsonov, A. V. ; Larionova, Yu O. ; Egorova, S. V. ; Savatenkov, V. M. / The 2405 Ma doleritic dykes in the Karelian Craton : A fragment of a Paleoproterozoic large igneous province. In: Doklady Earth Sciences. 2017 ; Vol. 472, No. 1. pp. 72-77.

BibTeX

@article{0e2bdaa5e5dd4fe69c718b1c3afa9a9e,
title = "The 2405 Ma doleritic dykes in the Karelian Craton: A fragment of a Paleoproterozoic large igneous province",
abstract = "New data on the age and composition of doleritic dykes of the Karelian Craton on the Fennoscandian Shield are reported. Based on the results of U–Pb dating of baddeleyite, a new age episode (2404 ± 5 Ma) in the formation of basic rocks on the Karelian Craton is established. Comparison of the composition of the studied dolerite with that of dykes of the same age from other Archean cratons worldwide shows their essential similarity and allows us to suggest their formation within a single large igneous province. The data obtained support the current models of supercontinental reconstructions for the period of 2400 Ma.",
author = "Stepanova, {A. V.} and Salnikova, {E. B.} and Samsonov, {A. V.} and Larionova, {Yu O.} and Egorova, {S. V.} and Savatenkov, {V. M.}",
year = "2017",
month = jan,
day = "1",
doi = "10.1134/S1028334X17010196",
language = "English",
volume = "472",
pages = "72--77",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "1",

}

RIS

TY - JOUR

T1 - The 2405 Ma doleritic dykes in the Karelian Craton

T2 - A fragment of a Paleoproterozoic large igneous province

AU - Stepanova, A. V.

AU - Salnikova, E. B.

AU - Samsonov, A. V.

AU - Larionova, Yu O.

AU - Egorova, S. V.

AU - Savatenkov, V. M.

PY - 2017/1/1

Y1 - 2017/1/1

N2 - New data on the age and composition of doleritic dykes of the Karelian Craton on the Fennoscandian Shield are reported. Based on the results of U–Pb dating of baddeleyite, a new age episode (2404 ± 5 Ma) in the formation of basic rocks on the Karelian Craton is established. Comparison of the composition of the studied dolerite with that of dykes of the same age from other Archean cratons worldwide shows their essential similarity and allows us to suggest their formation within a single large igneous province. The data obtained support the current models of supercontinental reconstructions for the period of 2400 Ma.

AB - New data on the age and composition of doleritic dykes of the Karelian Craton on the Fennoscandian Shield are reported. Based on the results of U–Pb dating of baddeleyite, a new age episode (2404 ± 5 Ma) in the formation of basic rocks on the Karelian Craton is established. Comparison of the composition of the studied dolerite with that of dykes of the same age from other Archean cratons worldwide shows their essential similarity and allows us to suggest their formation within a single large igneous province. The data obtained support the current models of supercontinental reconstructions for the period of 2400 Ma.

UR - http://www.scopus.com/inward/record.url?scp=85017573225&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17010196

DO - 10.1134/S1028334X17010196

M3 - Article

AN - SCOPUS:85017573225

VL - 472

SP - 72

EP - 77

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 52350401